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Schofield, P. F., Knight, K. S., Covey-Crump, S. J., Cressey, G., Stretton, I. C. (2002) Accurate quantification of the modal mineralogy of rocks when image analysis is difficult. Mineralogical Magazine, 66 (1) 189-200 doi:10.1180/0026461026610022

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Reference TypeJournal (article/letter/editorial)
TitleAccurate quantification of the modal mineralogy of rocks when image analysis is difficult
JournalMineralogical Magazine
AuthorsSchofield, P. F.Author
Knight, K. S.Author
Covey-Crump, S. J.Author
Cressey, G.Author
Stretton, I. C.Author
Year2002 (February)Volume66
Issue1
PublisherMineralogical Society
DOIdoi:10.1180/0026461026610022Search in ResearchGate
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Mindat Ref. ID243334Long-form Identifiermindat:1:5:243334:3
GUID0
Full ReferenceSchofield, P. F., Knight, K. S., Covey-Crump, S. J., Cressey, G., Stretton, I. C. (2002) Accurate quantification of the modal mineralogy of rocks when image analysis is difficult. Mineralogical Magazine, 66 (1) 189-200 doi:10.1180/0026461026610022
Plain TextSchofield, P. F., Knight, K. S., Covey-Crump, S. J., Cressey, G., Stretton, I. C. (2002) Accurate quantification of the modal mineralogy of rocks when image analysis is difficult. Mineralogical Magazine, 66 (1) 189-200 doi:10.1180/0026461026610022
Abstract/NotesAbstractThe volume proportions of the mineral phases in two strongly deformed olivine-orthopyroxene rocks have been quantified by whole-pattern stripping of fixed geometry X-ray powder diffraction data. The results were compared with the phase proportions as determined by Rietveld refinement of time-of-flight neutron powder diffraction data, and were shown to be in excellent agreement. The X-ray technique not only provides a very rapid and cost-effective method of determining phase proportions, but it also circumvents several of the problems associated with obtaining this information by image analysis. Moreover, the technique is particularly advantageous in strongly textured rocks or in rocks that contain significant residual strains. As such it offers a powerful technique for analysing the mineralogical composition of fine-grained and/or deformed experimental run products, which makes it of considerable potential for monitoringin situthe progress of mineral reactions during laboratory experiments.


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